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Each depth interval was divided into four sections, homogenized and analyzed independently.
We therefore standardized species observations in each depth interval by applying a multiplier equal to the average dive time in the most heavily sampled depth interval divided by the average dive time in each respective interval.
At each depth interval sampled, the salinity increased between water table rise and fall.
Significant vadose zone biodegradation over a relatively small depth interval was observed.
To create a hypsometric curve for each individual reef, the percentage of each one meter depth interval is determined using their calculated surface area.
Sampling effort (dive time) across each 10-m depth interval was relatively uniform across most depths, but somewhat shorter at the deepest intervals.
A TWT (two-way travel time) interval of 0.1 s corresponds approximately to a water depth interval of 75 m or a sediment interval of 100 m.
Predicted measurements at the monitoring zones covering a depth interval between 1950 m and 2120 m are analyzed.
The lowest CSV of −43 kPa was obtained under single line design within the 0 40 cm soil depth interval.
Soil strength was measured with a self-recording penetrometer at soil depth interval of 2.5 50 cm depth.
In the 60 100 cm depth interval, topographic wetness index was the most important parameter used in regression tree model.
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CEO of Professional Science Editing for Scientists @ prosciediting.com